Base-level Fluctuation
Base-Level Fluctuation is a geological process denoting oscillations in the elevation of a reference surface that governs the position and movement of sedimentary deposition and erosion boundaries, distinguishing it from static or tectonically driven controls by reflecting changes in the balance between accommodation space and sediment supply in sequence stratigraphy.
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Chris Paola, Jim Mullin, Chris Ellis et al. · GSA Today · 2001 · 114 citations · Full text
Francesco Latino Chiocci, Gemma Ercilla, Jun Cyric Shane S. Dela Torre · Sedimentary Geology · 1997 · 100 citations
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University of Liverpool
Liverpool, United Kingdom
2 h-index
3 publications
152 citations
Institute for the Dynamics of Environmental Processes
Mestre, Italy
1 h-index
1 publications
100 citations
University of Colorado Boulder
Boulder, United States
1 h-index
1 publications
69 citations
Ifremer
Brest, France
1 h-index
1 publications
100 citations
Laboratoire Méditerranéen de Préhistoire Europe Afrique
Aix-en-Provence, France
1 h-index
1 publications
26 citations
Universidade Federal do Rio Grande do Norte
Natal, Brazil
1 h-index
3 publications
81 citations
Tokyo University of Pharmacy and Life Sciences
Hachiōji, Japan
1 h-index
1 publications
27 citations
University of California, Davis
Davis, United States
1 h-index
1 publications
10 citations
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6 publications · 297 citations
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2 publications · 100 citations
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2 publications · 133 citations
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2 publications · 110 citations
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